| Basic Information | Biotope classification | Ecology | Habitat preferences and distribution | Species composition | Sensitivity | Importance |
LR.FLR.Rkp.H recorded (
) and expected (
) distribution in Britain and Ireland (see below)
This biotope is dominated by species able to withstand the frequent disturbance caused by wave action. The fact that LR.H rockpools are shallow and have a mixed substratum means that sand and pebbles will be frequently moved around the rockpool. This is especially true in stormy weather when larger cobbles and boulders may be moved into the pool and when the pool may be flushed clean of sediment. This in itself means that the community is unlikely to be a climax community, but more a transient community dominated by ephemeral, rapidly growing species that are able quickly to dominate space created by wave energy. Furthermore, both the flora and fauna are likely to vary both spatially, i.e. between rock pools, and on a temporal basis, depending on the frequency, severity and timing of disturbance.Primary producers in this biotope are represented by ephemeral green algae such as Ulva sp. Ulva intestinalis can grow rapidly and is tolerant of a range of temperatures and salinities. Ulva intestinalis is also the preferred food of Littorina littorea (see below).
In terms of characterizing species, suspension feeders are the dominant trophic group in LR.H. The most common suspension feeders likely to be found in LR.H are the hydroid Obelia longissima and the common mussel Mytilus edulis. The acorn barnacle Semibalanus balanoides may also be common. Semibalanus balanoides actively feeds on detritus and zooplankton. Mytilus edulis actively feeds on bacteria, phytoplankton, detritus, and dissolved organic matter (DOM). Obelia longissima is a passive suspension feeder, feeding on small zooplankton, small crustaceans, oligochaetes, insect larvae and probably detritus. The branches of Obelia longissima may be used as substratum by Mytilus edulis pediveligers (Brault & Bourget, 1985). Other suspension feeders may include the barnacle Elminius modestus and the tubeworm Pomatoceros triqueter.
The grazing gastropod Littorina littorea feeds on range of fine red, green and brown algae including Ulva sp., Cladophora sp. and Ectocarpus sp.
Deposit feeding worms such as the sand mason Lanice conchilega and the lugworm Arenicola marina may be found if patches of sand are present in the pools. The sand mason is also capable of active suspension feeding.
The common shore crab Carcinus maenas is the largest mobile predator frequently associated with LR.H. Carcinus maenas is likely to move in and out of the rockpool feeding on plant and animal material including Semibalanus balanoides and Littorina littorea.
Rockpools constitute a distinct environment for which physiological adaptations by the flora and fauna may be required (Lewis, 1964). Conditions within rockpools are the consequence of prolonged separation from the main body of the sea, and physico-chemical factors within them fluctuate dramatically (Huggett & Griffiths, 1986). Shallow pools such as those associated with LR.H are especially influenced by insolation, air temperature and rainfall, the effects of which become more significant towards the high shore, where pools may be isolated from the sea for a number of days or weeks (Lewis, 1964).
Water temperature in pools follows the temperature of the air more closely than that of the sea. In summer, shallow pools are warmer by day, but may be colder at night, and in winter may be much colder than the sea (Pyefinch, 1943). It is also possible that shallow pools may freeze over in the coldest winter months.High air temperatures cause surface evaporation of water from pools, so that salinity steadily increases, especially in pools not flooded by the tide for several days. Alternatively, high rainfall will reduce pool salinity or create a surface layer of brackish/nearly fresh water for a period. The extent of temperature and salinity change is affected by the frequency and time of day at which tidal inundation occurs. If high tide occurs in early morning and evening the diurnal temperature follows that of the air, whilst high water at midday suddenly returns the temperature to that of the sea (Pyefinch, 1943). Heavy rainfall, followed by tidal inundation can cause dramatic fluctuations in salinity, and values ranging from 5-30 psu have been recorded in rockpools over a period of 24 hrs (Ranade, 1957). Rockpools in the supralittoral, littoral fringe and upper eulittoral are liable to gradually changing salinities followed by days of fully marine or fluctuating salinity at times of spring tide (Lewis, 1964).
Due to the frequent disturbances likely to affect this biotope, any seasonal changes are likely to be masked by changes caused by wave energy. Some species of hydroids demonstrate seasonal cycles of growth in spring/summer and regression (die back) in late autumn/winter, over wintering as dormant stages or juvenile stages (Gili & Hughes, 1995). Many hydroids are opportunists adapted to rapid growth and reproduction (r-selected), taking advantage of the spring/summer phytoplankton bloom and more favourable (less stormy) conditions (Gili & Hughes, 1995). Brault & Bourget (1985) noted that Obelia longissima exhibited an annual cycle of biomass, measured as colony length, on settlement plates in the St Lawrence estuary. Colony length increased from settlement in June, reaching a maximum in November to March and then decreasing again until June, although the decline late in the year was attributed to predation, and data was only collected over a two year period. The ephemeral algae are also likely to experience an obvious decline in biomass over the winter months.This review can be cited as follows:
Marshall, C.E. 2005. Hydroids, ephemeral seaweeds and Littorina littorea in shallow eulittoral mixed substrata pools. Marine Life Information Network: Biology and Sensitivity Key Information Sub-programme [on-line]. Plymouth: Marine Biological Association of the United Kingdom. [cited 21/05/2013]. Available from: <http://www.marlin.ac.uk/habitatecology.php?habitatid=54&code=2004>